Pan Hongyi, Song Qize, Yi Luyao, Li Bo, Bi Rutian
College of Resources and Environment, Shanxi Agricultural University, Taigu, China.
Datong Daylily Industrial Development Research Institute, Datong, China.
PLoS One. 2025 May 8;20(5):e0323065. doi: 10.1371/journal.pone.0323065. eCollection 2025.
It is imperative to promote water-saving irrigation technology and develop newly cultivated land in the Loess Plateau. This study focused on the interaction between roots and soil to examine the effects of different amounts of irrigation on soil structure of newly cultivated land. Herein, five irrigation levels were set, i.e., sufficient irrigation (W100), mild deficit irrigation (W80), moderate deficit irrigation (W60), severe deficit irrigation (W40), and rain-fed (RF). Physical properties and structural stability indexes of the rhizosphere soil were measured, and their relationship with plant root morphology were analyzed. The results showed that the soil structure under the high irrigation amount group (W80 and W100) was relatively stable. The average particle density of soil in each plot decreased significantly after the experiment, while the soil total porosity remained unchanged in W80 and W100 treatments. The proportion of large aggregates, the mean weight diameter, and the geometric mean diameter of soil significantly reduced in the low irrigation amount group (RF, W40, and W60). In contrast, the W100 and W80 treatments inhibited the decline in soil aggregate stability. Change in the generalized soil structure index (GSSI) and soil three-phase structure distance (STPSD) of W100 and W80 treatments were not significant, before and after the experiment. These results suggested that the soil in newly cultivated land treated with sufficient and mild deficit irrigation was closer to the ideal state for crops growing. Path analysis identified the average soil moisture content had the greatest negative effect on STPSD primarily through the root length, root surface area, and root dry weight. In conclusion, irrigation amount occupies a dominant position among all factors influencing soil structure considered in the study. And the mild deficit irrigation is suitable for agricultural cultivation in the Loess Plateau area, from the soil structure protection and water-saving perspectives.
推广节水灌溉技术和开发黄土高原新耕地势在必行。本研究聚焦于根系与土壤的相互作用,以考察不同灌溉量对新耕地土壤结构的影响。在此,设置了五个灌溉水平,即充分灌溉(W100)、轻度亏缺灌溉(W80)、中度亏缺灌溉(W60)、重度亏缺灌溉(W40)和雨养(RF)。测定了根际土壤的物理性质和结构稳定性指标,并分析了它们与植物根系形态的关系。结果表明,高灌溉量组(W80和W100)的土壤结构相对稳定。实验后各小区土壤的平均颗粒密度显著降低,而W80和W100处理下土壤总孔隙度保持不变。低灌溉量组(RF、W40和W60)土壤大团聚体比例、平均重量直径和几何平均直径显著降低。相比之下,W100和W80处理抑制了土壤团聚体稳定性的下降。实验前后,W100和W80处理的广义土壤结构指数(GSSI)和土壤三相结构距离(STPSD)变化不显著。这些结果表明,充分灌溉和轻度亏缺灌溉处理的新耕地土壤更接近作物生长的理想状态。通径分析表明,平均土壤含水量主要通过根长、根表面积和根干重对STPSD产生最大的负效应。总之,在本研究考虑的影响土壤结构的所有因素中,灌溉量占主导地位。从土壤结构保护和节水角度来看,轻度亏缺灌溉适合黄土高原地区的农业种植。